Mountains

The Himalayas are known as the roof of the world. They are the highest mountain range in the world, home to the highest peak, Mount Everest.

Yes, there are lots of mountains on the moon, as proved by Italian professor of Mathematics, Galileo. The proved this by making the first 20x zoom telescope and noticing mounting-looking hills, later realizing they were in fact mountains, measuring about 2.5 miles high. To compare, Mount Everest is 3 miles high.

The summit of a mountain is the highest point or peak of the mountain where the elevation is greatest. It is often a goal for climbers to reach the summit of a mountain as a significant achievement.

Yes, the Rocky Mountains are known for having steep terrain in many areas, especially along their western slopes. The range features rugged peaks, deep valleys, and sheer cliffs, making for challenging hiking, climbing, and skiing opportunities.

Mountains that are snow covered even in the summer typically have high elevations, which means that temperatures are colder at those heights. This prevents the snow from melting, leading to year-round snow coverage. Additionally, the slopes of these mountains may be angled in a way that prevents sunlight from reaching the snow, keeping it frozen.

Sunspots appear dark in color because they are cooler than the surrounding areas on the Sun's surface, which are much hotter. The cooler temperature of sunspots is due to magnetic activity inhibiting the flow of heat from deeper within the Sun.

James Irwin is that former astronaut. A link is provided.

The Mount Meakan eruption in 1929 resulted in the deaths of at least 3 people.

Fog frequently forms in mountainous regions due to air being forced upwards by the mountains themselves. This causes the air to cool and condense its moisture into fog and clouds. This is called orographic fog.

Bulbs can be dimmer than others due to differences in wattage, age, or type of bulb. Lower wattage bulbs will produce less light output, while older bulbs may lose brightness over time. Different types of bulbs, such as incandescent, LED, or CFL, also have varying levels of brightness.

The sea level of a mountain can be determined using GPS technology to measure the elevation of the mountain's peak above sea level. Additionally, topographic maps and online platforms provide elevation data for specific locations.

The biggest mountain outside of Earth is Olympus Mons, a giant shield volcano on Mars. It is about 13.6 miles (22 kilometers) high, making it the tallest known volcano and mountain in the entire solar system.

Andes - continental oceanic

aleutians - oceanic oceanic

North American cordillera - arc continent

Appalachians - continental continental

When a range of mountains is tens to hundreds of kilometers in length and width, and is near an active tectonic plate boundary or coast, it is called a mountain range.

Fault block mountains are formed by the uplifting and tilting of large blocks of the Earth's crust along fault lines, usually due to tensional forces pulling the blocks apart. Orogeny, on the other hand, refers to the process of mountain building typically caused by the collision of tectonic plates, resulting in the folding, faulting, and uplifting of rock layers. The forces generating orogeny are compressional, as opposed to the tensional forces that create fault block mountains.

The block on the right is most likely moving upward relative to the block on the left due to tectonic forces, but erosion acts independently of tectonic movement. Erosion can lower the elevation of a block over time through processes like weathering, mass wasting, and transport of sediment, regardless of its tectonic movement.

Mountains are found in Earth's lithosphere, specifically in the crustal layer composed of rocks. They can be formed by tectonic activity, such as the collision of tectonic plates, or by volcanic activity.

You are lava. Lava is molten rock that flows as a liquid when hot and solidifies to form mountains when cooled. It can erupt from volcanoes to destroy towns and often resides underground in magma chambers.

Precipitation occurs on the windward side of mountain ranges because as moist air is forced to rise over the mountains, it cools, causing the air to reach its dew point and release moisture in the form of rain or snow. This process, known as orographic lifting, is responsible for the higher levels of precipitation on the windward side compared to the leeward side of the mountains.

Himalayan salt is mined from the Khewra Salt Mine in Pakistan, which is located at the western edge of the Himalayas. The salt is typically hand-mined and extracted from rock salt deposits that have been forming for millions of years.

Two mountains that can coexist without affecting each other are Mount Everest and K2. They are located in different regions (Himalayas and Karakoram) and are far enough apart that they do not have any direct impact on each other's geological processes.

The mountains of the Basin and Range province formed from extensional tectonic forces that caused the Earth's crust to stretch and thin out, resulting in horst and graben structures. This extensional tectonics created alternating blocks of uplifted mountains and down-dropped valleys, giving the region its characteristic basin-and-range topography.

Forces from tectonic plate movement can create folded mountains when two plates collide and compress, causing rocks to fold and buckle. Block mountains form when tectonic plates slide past each other, creating faults that lift blocks of land. Volcanic mountains are built from magma rising through the Earth's crust at plate boundaries or hot spots, accumulating layers of volcanic material over time.

They erode by the effects of wind and water

One clue that a mountain is young is if it has sharp, jagged peaks and steep slopes. This indicates that the mountain has undergone recent tectonic activity, such as uplift or faulting. In contrast, an old mountain would have more rounded peaks and gentle slopes due to erosion over time.